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NOAA Research on Hyperspectral Trace Gas Retrievals

Explore the role of hyperspectral sensing from satellites for operational meteorology, atmospheric chemistry, and climate monitoring. Current and future applications discussed with a focus on trace gases and air quality predictions.

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NOAA Research on Hyperspectral Trace Gas Retrievals

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  1. The Use of Current and Future Hyperspectral Trace Gas Retrievals in Atmospheric Chemistry Research at NOAA R. Bradley Pierce NOAA/NESDIS/STAR Collaborators: Todd Schaack and Allen Lenzen (UW-Madison, SSEC) Jay Al-Saadi and MuraliNatarajan (NASA-LaRC) Bill Smith (Hampton University) Data Providers: Steve Wofsy (Harvard), RuShanGao, Ryan Spackman, David.W.Fahey (NOAA/ESRL), Chris Boone (University of Waterloo), Kevin Bowman, Nathaniel Livesey (NASA/JPL), PawanBartia (NASA/GSFC), Anne Thompson (PSU)

  2. Question 13: What are the views of NOAA Research on the role of present, emerging, and future hyperspectral sensing from satellite for operational meteorology, atmospheric chemistry, and climate monitoring (in particular trace gases)? Current: Assimilation of hyperspectral trace gas retrievals within global chemical data assimilation systems canbe used to constrain background tropospheric ozone distributions and improve regional Air Quality (AQ) predictions. - TES/OMI/MLS 2006 data denial studies during TEXAQS Future: Assimilation of hyperspectral trace gas retrievals within global chemical data assimilation systemsshouldbe used to constrain radiativelyactive trace gas distributions and improve forward modeling for radiance assimilation. - ACE/IASI 2010 GHG validation during HIPPO-3 Pierce, R. B., et al. (2007) Chemical data assimilation estimates of continental US ozone and nitrogen budgets during the Intercontinental Chemical Transport Experiment-North America. J. Geophys. Res. doi:10.1029/2006JD007722

  3. Question 13: What are the views of NOAA Research on the role of present, emerging, and future hyperspectral sensing from satellite for operational meteorology, atmospheric chemistry, and climate monitoring (in particular trace gases)? Current: Assimilation of hyperspectral trace gas retrievals within global chemical data assimilation systems canbe used to constrain background tropospheric ozone distributions and improve regional Air Quality (AQ) predictions. - TES/OMI/MLS 2006 data denial studies during TEXAQS Future: Assimilation of hyperspectral trace gas retrievals within global chemical data assimilation systemsshouldbe used to constrain radiativelyactive trace gas distributions and improve forward modeling for radiance assimilation. - ACE/IASI 2010 GHG validation during HIPPO-3 Pierce, R. B., et al. (2007) Chemical data assimilation estimates of continental US ozone and nitrogen budgets during the Intercontinental Chemical Transport Experiment-North America. J. Geophys. Res. doi:10.1029/2006JD007722

  4. RAQMS 2006 Data Denial Study • Time period: August 2006 • Initial Conditions: July 15th, 2006 • (Baseline RAQMS OMI+TES ozone analysis) • Validation: 2006 IONS ozonesonde network (373 sondes) • Meteorological Analysis: GFS/GSI • Chemical Analysis: • Optimal Interpolation (IO) univariate (Pierce et al., 2007) • unified online troposphere/stratospheric chemistry for first guess • Procedure: • Compare RAQMS analyses with ozonesonde • No Assimilation • OMI (Cloud Cleared) only • TES (O3&CO) only • TES (O3&CO)+OMI (Cloud Cleared)

  5. RAQMS (2x2) 2006 OMI/TES Reanalysis O3/CO Assimilation Procedure Modeled O3+ OMI Obs Operator Modeled O3/CO+ TES Obs Operator Adjusted O3 Adjusted O3/CO First Guess Column First Guess Profile Column increment Local increment NOAA GFS Global Met RAQMS Global Met/Chem TES Profile Assimilation Cycle OMI Column Assimilation Cycle Pierce, R. B., et al. (2007) Chemical data assimilation estimates of continental US ozone and nitrogen budgets during the Intercontinental Chemical Transport Experiment-North America. J. Geophys. Res. doi:10.1029/2006JD007722

  6. August 2006 NO ASSIM Zonal mean CO/O3 (July 15, 2006 OMI+TES IC) RAQMS vs IONS

  7. August 2006 OMI Assim-NO ASSIM Zonal mean Delta CO/O3 (July 15, 2006 OMI+TES IC) Small (~2%) change in CO RAQMS vs IONS +15-20%

  8. August 2006 TES Assim-NO ASSIM Zonal mean Delta CO/O3 (July 15, 2006 OMI+TES IC) RAQMS vs IONS (+/-) 15-20% change in (NH/SH) +15-20%

  9. Pierce, R. B., et al., 2009 Impacts of background ozone production on Houston and Dallas, TX Air Quality during the TexAQS field mission, J. Geophys. Res., 114, D00F09, doi:10.1029/2008JD011337

  10. Pierce, R. B., et al., 2009 Impacts of background ozone production on Houston and Dallas, TX Air Quality during the TexAQS field mission, J. Geophys. Res., 114, D00F09, doi:10.1029/2008JD011337

  11. Pierce, R. B., et al., 2009 Impacts of background ozone production on Houston and Dallas, TX Air Quality during the TexAQS field mission, J. Geophys. Res., 114, D00F09, doi:10.1029/2008JD011337

  12. Pierce, R. B., et al., 2009 Impacts of background ozone production on Houston and Dallas, TX Air Quality during the TexAQS field mission, J. Geophys. Res., 114, D00F09, doi:10.1029/2008JD011337

  13. Impact of Global BC on regional AQ Prediction Analyzed Eastern Pacific O3 Analyzed Eastern Pacific CO Assessment using pre-operational NOAA/NWS NAM-CMAQ 12km forecast (July 21-August 5, 2006) RAQMS lateral Boundary Conditions lead to 10-15 ppbv reductions in off-shore surface ozone and 5-10 ppbv increases in surface ozone over mountain regions of the western US. Mean O3 Difference (ppbv) (RAQMS-BC – Fixed-BC) Comparison with EPA AIRNow surface ozone west of -115oW shows improved slope and correlations but increased positive bias. NAM-CMAQ vs AIRNOW Static BC RAQMS BC Mean O3 biases (ppbv) Tang. Y., et al., (2008), The impact of chemical lateral boundary conditions on CMAQ predictions of tropospheric ozone over the continental United States, Environmental Fluid Mechanics, DOI: 0.1007/s10652-008-9092-5

  14. Question 13: What are the views of NOAA Research on the role of present, emerging, and future hyperspectral sensing from satellite for operational meteorology, atmospheric chemistry, and climate monitoring (in particular trace gases)? Current: Assimilation of hyperspectral trace gas retrievals within global chemical data assimilation systems canbe used to constrain background tropospheric ozone distributions and improve regional Air Quality (AQ) predictions. - TES/OMI/MLS 2006 data denial studies during TEXAQS Future: Assimilation of hyperspectral trace gas retrievals within global chemical data assimilation systemsshouldbe used to constrain radiativelyactive trace gas distributions and improve forward modeling for radiance assimilation. - ACE/IASI 2010 GHG validation during HIPPO-3 Pierce, R. B., et al. (2007) Chemical data assimilation estimates of continental US ozone and nitrogen budgets during the Intercontinental Chemical Transport Experiment-North America. J. Geophys. Res. doi:10.1029/2006JD007722

  15. Radiative influences of Trace Gases Radiative influences of Ozone, CO, CH4, CO2, N2O and other GHG are significant Temporal/spatial variability should be accounted for in forward radiative transfer modeling Figure provided by Tim Schmit, NESDIS/STAR

  16. Radiative influences of Trace Gas Trends From Forster, P., et al. 2007: Changes in Atmospheric Constituents and in Radiative Forcing. In: Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change Trends in stratospheric Ozone and GHG concentrations largely account for observed stratospheric temperature trends From Shine, K., et al., (2003), A comparison of model-simulated trends in stratospheric temperatures, Q. J. R. Meteorol. Soc. (2003), 129, pp. 1565–1588 doi: 10.1256/qj.02.186

  17. Atmospheric Chemistry Experiment (ACE) PI Peter Bernath, University of Waterloo, Ontario Canada Solar Occultation Infrared Fourier Transform Spectrometer Using Version 2.2 data FTS Species MINOR GASES CO2, CO, H2O, O3, N2O, CH4 TRACE GASES Nitrogen species NH3, NO, NO2, N2O5, HNO2, HNO3,HO2NO2, HCN Hydrogen Species H2CO, H2CO2, HDO, H2 Halogens CCl3F (F11), CCl2F2 (F12), CH3CCl3, CHClF2 (F22), CH3Cl, CCl4, SF6, HF, HCl, CF2O, ClONO2, HOCl Sulfur oxides OCS, SO2 Other species C2H2, C2H4, C2H6, CH3D As well as aerosols and PSC IR spectra ACE sampling pattern

  18. RAQMS (2x2) 2010 OMI/MLS Real-time O3 Assimilation Procedure Modeled O3+ OMI Obs Operator Modeled O3 Adjusted O3 Adjusted O3 First Guess Column First Guess Profile Column increment Local increment NOAA GFS Global Met RAQMS Global Met/Chem MLS Profile Assimilation Cycle OMI Column Assimilation Cycle

  19. ACE/RAQMS 800K O3 March 01-April 04, 2010 Southern Hemisphere Northern Hemisphere

  20. ACE vs RAQMS O3 March 01-April 04, 2010 Southern Hemisphere Northern Hemisphere ACE QC: error<10% RAQMS shows Low bias in NH lower stratosphere relative to ACE

  21. High-performance Instrumented Airborne Platform for Environmental Research (HIAPER), Pole-to-Pole Observation (HIPPO) III PI: Steven C. Wofsy, Harvard University NCAR G-V aircraft March 20-April 20, 2010 National Science Foundation (NSF)-sponsored effort to study the distribution of greenhouse gases and black carbon in the atmosphere. High-accuracy measurements of greenhouse gases and black carbon particles from the top of the troposphere to the earth's surface and pole-to-pole. http://www.eol.ucar.edu/deployment/field-deployments/field-projects/hippo_global_3

  22. Anchorage to Hilo 03/29/2010 RAQMS 320K O3 with HIPPO 3 Flight Track RAQMS O3 curtain with HIPPO 3 insitu O3 (Spackman, NOAA/ESRL)

  23. ACE/HIPPO vs RAQMS O3 March 01-April 16, 2010 Southern Hemisphere Northern Hemisphere RAQMS shows high bias in tropical and subtropical upper troposphere relative to HIPPO RAQMS shows high bias in tropical and subtropical upper troposphere relative to HIPPO RAQMS shows Low bias in NH lower stratosphere relative to ACE & HIPPO

  24. ACE O3 vs CH4 Pacific Sector (120E-120W) March 24-April 16, 2010 Southern Hemisphere Northern Hemisphere QC: error<10%

  25. ACE & HIPPO O3 vs CH4 Pacific Sector (120E-120W) March 24-April 16, 2010 Southern Hemisphere Northern Hemisphere Remarkable Agreement with HIPPO insitu measurements! QC: error<10%

  26. ACE & HIPPO & RAQMS O3 vs CH4 Pacific Sector (120E-120W) March 24-April 16, 2010 Southern Hemisphere Northern Hemisphere Missing CH4/CO/CO2 photochemistry Missing CH4/CO/CO2 photochemistry Brewer Dobson Circulation Brewer Dobson Circulation Surface boundary condition Surface boundary condition

  27. ACE O3 vs N2O Pacific Sector (120E-120W) March 24-April 16, 2010 Southern Hemisphere Northern Hemisphere QC: error<10%

  28. ACE & HIPPO O3 vs N2O Pacific Sector (120E-120W) March 24-April 16, 2010 Southern Hemisphere Northern Hemisphere Remarkable Agreement with HIPPO insitu measurements! QC: error<10%

  29. ACE & HIPPO & RAQMS O3 vs N2O Pacific Sector (120E-120W) March 24-April 16, 2010 Southern Hemisphere Northern Hemisphere Brewer Dobson Circulation Brewer Dobson Circulation Surface boundary condition Surface boundary condition

  30. ACE O3 vs CO Pacific Sector (120E-120W) March 24-April 16, 2010 Southern Hemisphere Northern Hemisphere QC: error<10%

  31. ACE & HIPPO O3 vsCO Pacific Sector (120E-120W) March 24-April 16, 2010 Southern Hemisphere Northern Hemisphere Remarkable Agreement with HIPPO insitu measurements! QC: error<10%

  32. ACE & HIPPO & RAQMS O3 vsCO Pacific Sector (120E-120W) March 24-April 16, 2010 Southern Hemisphere Northern Hemisphere Brewer Dobson Circulation Brewer Dobson Circulation Overestimate in UT/LS Good agreement in free troposphere

  33. ACE & HIPPO & RAQMS & IASI O3 vsCO Pacific Sector (120E-120W) March 24-April 16, 2010 Southern Hemisphere Northern Hemisphere Retrieved O3 r= 0.962165 Median Bias= -0.00191106 ppmv Retrieved CO r= 0.0679334 Median Bias= -19.5601 ppbv RAQMS CO r= 0.0444996 Median Bias= -23.2552 ppbv RAQMS at coincident ACE and IASI points along HIPPO flight Track

  34. Anchorage to Hilo 03/29/2010 HIPPO 3 insituvs RAQMS O3/CO RAQMS O3 curtain with HIPPO 3 insitu O3 (Spackman, NOAA/ESRL) RAQMS CO curtain with HIPPO 3 insituCO (Wofsy, Harvard)

  35. Anchorage to Hilo 03/29/2010 HIPPO 3 insituvs IASI O3/CO IASI (Smith, HU) O3 curtain with HIPPO 3 insitu O3 (Spackman, NOAA/ESRL) IASI (Smith, HU) CO curtain with HIPPO 3 insituCO (Wofsy, Harvard)

  36. Summary: • Current: Assimilation of hyperspectral trace gas retrievals within global chemical data assimilation systems canbe used to constrain background tropospheric ozone distributions and improve regional Air Quality (AQ) predictions. • Future: Assimilation of hyperspectral trace gas retrievals within global chemical data assimilation systemsshouldbe used to constrain radiativelyactive trace gas distributions and improve forward modeling for radiance assimilation. • But Operational models need to predict both tropospheric and stratospheric chemistry (e.g. GMES/MACC)! • And we need to downlink full resolution JPSS CrIS spectra for GHG retrieval! • Proposed next generation Hyperspectral Sounder (IASI NG, 2 x radiometric and 2 x spectral Resolution, 2018+) and Solar Limb Occultation (Solar Occultation for Atmospheric Research, SOAR, 3x vertical resolution, 2016+) would provide improved trace gas retrievals for Weather, Air Quality and Climate applications.

  37. ACE & HIPPO & RAQMS & IASI O3 vsCH4 Pacific Sector (120E-120W) March 24-April 16, 2010 Southern Hemisphere Northern Hemisphere RAQMS at coincident ACE and IASI points along HIPPO flight Track

  38. ACE & HIPPO & RAQMS & IASI O3 vsN2O Pacific Sector (120E-120W) March 24-April 16, 2010 Southern Hemisphere Northern Hemisphere RAQMS at coincident ACE and IASI points along HIPPO flight Track RAQMS at coincident ACE and IASI points along HIPPO flight Track

  39. 03/27 Final Stats with respect to HIPPO insitu measurements Retrieved O3 r= 0.962165, Median Bias= -0.00191106 RAQMS O3 r= 0.971285, Median Bias= -0.00144393 Retrieved CO r= 0.0679334, Median Bias= -19.5601 RAQMS CO r= 0.0444996, Median Bias= -23.2552 Retrieved CH4 r= 0.136063, Median Bias= 0.0558940 RAQMS CH4 r= 0.108257, Median Bias= 0.0565929 Retrieved N2O r= 0.164484, Median Bias= 16.6093 RAQMS N2O r= 0.166612, Median Bias= 16.3700

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